Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea

This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, s...
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Autor*in:	Adem Akpınar [verfasserIn] Halid Jafali [verfasserIn] Eugen Rusu [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	renewable energy wave power temporal variation hourly variation trend Black Sea

Übergeordnetes Werk:	In: Sustainability - MDPI AG, 2009, 11(2019), 3, p 562
Übergeordnetes Werk:	volume:11 ; year:2019 ; number:3, p 562

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/su11030562

Katalog-ID:	DOAJ075862514

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spelling	10.3390/su11030562 doi (DE-627)DOAJ075862514 (DE-599)DOAJ459f921a52e04f1a80863ba9a05cf1b8 DE-627 ger DE-627 rakwb eng TD194-195 TJ807-830 GE1-350 Adem Akpınar verfasserin aut Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations. renewable energy wave power temporal variation hourly variation trend Black Sea Environmental effects of industries and plants Renewable energy sources Environmental sciences Halid Jafali verfasserin aut Eugen Rusu verfasserin aut In Sustainability MDPI AG, 2009 11(2019), 3, p 562 (DE-627)610604120 (DE-600)2518383-7 20711050 nnns volume:11 year:2019 number:3, p 562 https://doi.org/10.3390/su11030562 kostenfrei https://doaj.org/article/459f921a52e04f1a80863ba9a05cf1b8 kostenfrei https://www.mdpi.com/2071-1050/11/3/562 kostenfrei https://doaj.org/toc/2071-1050 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2507 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 11 2019 3, p 562
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allfieldsGer	10.3390/su11030562 doi (DE-627)DOAJ075862514 (DE-599)DOAJ459f921a52e04f1a80863ba9a05cf1b8 DE-627 ger DE-627 rakwb eng TD194-195 TJ807-830 GE1-350 Adem Akpınar verfasserin aut Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations. renewable energy wave power temporal variation hourly variation trend Black Sea Environmental effects of industries and plants Renewable energy sources Environmental sciences Halid Jafali verfasserin aut Eugen Rusu verfasserin aut In Sustainability MDPI AG, 2009 11(2019), 3, p 562 (DE-627)610604120 (DE-600)2518383-7 20711050 nnns volume:11 year:2019 number:3, p 562 https://doi.org/10.3390/su11030562 kostenfrei https://doaj.org/article/459f921a52e04f1a80863ba9a05cf1b8 kostenfrei https://www.mdpi.com/2071-1050/11/3/562 kostenfrei https://doaj.org/toc/2071-1050 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2507 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 11 2019 3, p 562
allfieldsSound	10.3390/su11030562 doi (DE-627)DOAJ075862514 (DE-599)DOAJ459f921a52e04f1a80863ba9a05cf1b8 DE-627 ger DE-627 rakwb eng TD194-195 TJ807-830 GE1-350 Adem Akpınar verfasserin aut Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations. renewable energy wave power temporal variation hourly variation trend Black Sea Environmental effects of industries and plants Renewable energy sources Environmental sciences Halid Jafali verfasserin aut Eugen Rusu verfasserin aut In Sustainability MDPI AG, 2009 11(2019), 3, p 562 (DE-627)610604120 (DE-600)2518383-7 20711050 nnns volume:11 year:2019 number:3, p 562 https://doi.org/10.3390/su11030562 kostenfrei https://doaj.org/article/459f921a52e04f1a80863ba9a05cf1b8 kostenfrei https://www.mdpi.com/2071-1050/11/3/562 kostenfrei https://doaj.org/toc/2071-1050 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2507 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 11 2019 3, p 562
language	English
source	In Sustainability 11(2019), 3, p 562 volume:11 year:2019 number:3, p 562
sourceStr	In Sustainability 11(2019), 3, p 562 volume:11 year:2019 number:3, p 562
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container_title	Sustainability
authorswithroles_txt_mv	Adem Akpınar @@aut@@ Halid Jafali @@aut@@ Eugen Rusu @@aut@@
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callnumber-first	T - Technology
author	Adem Akpınar
spellingShingle	Adem Akpınar misc TD194-195 misc TJ807-830 misc GE1-350 misc renewable energy misc wave power misc temporal variation misc hourly variation misc trend misc Black Sea misc Environmental effects of industries and plants misc Renewable energy sources misc Environmental sciences Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea
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topic	misc TD194-195 misc TJ807-830 misc GE1-350 misc renewable energy misc wave power misc temporal variation misc hourly variation misc trend misc Black Sea misc Environmental effects of industries and plants misc Renewable energy sources misc Environmental sciences
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title	Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea
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title_sort	temporal variation of the wave energy flux in hotspot areas of the black sea
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title_auth	Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea
abstract	This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations.
abstractGer	This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations.
abstract_unstemmed	This paper aims to examine the temporal variation of wave energy flux in the hotspot areas of the Black Sea. For this purpose, a 31-year long-term wave dataset produced by using a three-layered nested modelling system was used. Temporal variations of wave energy were determined at hourly, monthly, seasonal, and yearly basis at seventeen stations. Based on the results obtained, it can be concluded that the stations have very low fluctuations in mean wave power during the day. Mean wave power in the summer months shows a low difference between the stations, but in the winter months, there is a higher difference in wave power between the stations. This difference is more at the stations in the southwestern part of the Black Sea and much lower in the eastern Black Sea stations around Sinop, being in the middle of the southern coast of the Black Sea. In addition, it is concluded that mean wave energy flux presents a decreasing trend at all stations, but maximum wave power offers an increasing trend at most of the stations.
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Temporal Variation of the Wave Energy Flux in Hotspot Areas of the Black Sea

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